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Raman study of a highly
altered basalt -- AKB
igneous mineralogy, alteration
products, & a microorganism
| A Martian analog rock, a 1.1
billion-year-old Keweenawan basalt (AKB). This rock is a highly altered basalt
found in a creek. It has a fine-grained reddish matrix with small "clots"
of a grayish-green clay mineral and coarse amygdules filled with light-colored minerals. Two surfaces of this rock are studied: |
 |
 |
| heavily altered original surface, with
surface relief of several mm. |
roughly cut flat surface , unpolished. |
Mineral phases found in this rock:
 |
 |
 |
| The dark red matrix of the
altered basalt yielded spectra of hematite (alpha-Fe2O3), plagioclase, saponite, and
pyroxene. |
The mineral phases inside the large, white amygdules
are mainly calcite (CaCO3) and thomsonite (a type of zeolite). |
some rare phases --
microorganism, anatase, quartz, and K-feldspar |
Mineral distributions and mineral
proportions:
| Successive Raman spectra along two traverses cross from the
matrix to amygdules and back. |
Mineral modes obtained
based on automated traverses on the original and sawn surfaces |
 |
 |
 |
| Compare the two linear traverses, one with focus adjustment
at each point, one without. Basic mineral distributions are the same. |
Mineral modes obtained from the original surface |
Mineral modes obtained from the sawn surface |
Reference:
Wang A., Jolliff B. L., Haskin L. A., “Raman spectroscopic characterization of
a highly weathered basalt – igneous mineralogy, alteration products, and a
bug”, Twenty-ninth Lunar and Planetary Science Conference, 1998.
Wang A., Jolliff, B.L., and Haskin L.A. (1999) Raman spectroscopic
characterization of a highly weathered basalt: igneous mineralogy, alteration
products, and a microorganism, J. Geophys. Res., 104, 27067 -27077.

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